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We report the results of our recent experimental investigation which extends the search for magnetic ordering in the high-pressure, hcp phase of iron (ε-phase) to a temperature of 0.030 K. Mössbauer effect measurements were performed in the pressure range from atmospheric pressure to 21.5 GPa on a foil of natural iron (doped with 57Co). Measurements were made of the properties of both the α- and ε-phase constituents of the sample. No measurable magnetic hyperfine field was observed in the ε-phase from any of the spectra at pressures as high as 21.5 GPa and temperatures as low as 0.030 K.
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Cort et al. (1982) studied this question.
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